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COMPARATIVE ANALYSIS OF BIOMARKER HYDROCARBONS IN UPPERPROTEROZOIC, PALEOZOIC, AND MESOZOIC ORGANIC MATTEROF WEST SIBERIAKostyreva E.A., Fomin A.N.PP‐24Institution of Russian Academy of Sciences A.A. Trofimuk Institute of Petroleum Geology andGeophysics of the Siberian Branch RAS, Novosibirsk, Russia, KostyrevaEA@ipgg.nsc.ruIt has been identified that the saturated fractions of bitumens (chloroform extracts)from Upper Proterozoic, Paleozoic (Є‐C) and Mesozoic (J) deposits contain C 10 ‐C 37 n‐alkanes,C 13 ‐C 25 acyclic izoprenanes, cyclic biomarker hydrocarbons (HC) of sterane (C 21 ‐C 22 ) and C 27 ‐C 30 ) terpane (C 19 ‐C 35 ) series.The following biomarker parameters were established for Upper Proterozoic OM (wellVostok‐3): n‐C 27 /n‐C 17
PP‐24Pr/Ph1; tricyclane index
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Boreskov Institute of Catalysis of
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INTERNATIONAL SCIENTIFIC COMMITTEEA
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PLENARY LECTURES
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PL‐1first planetesimals (embryos
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PL‐2case the primary Earth substa
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PL‐310. If the high‐carbon rock
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PL‐5ON THE COMPLEXITY OF PRIMORDI
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MICROFOSSILS, BIOMOLECULES AND BIOM
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PL‐8MOLECULAR COLONIES AS A PRE
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PL‐9GENE NETWORKS AND THE EVOLUTI
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EMERGENT LIFE DRINKS ORDERLINESS FR
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PROTOBIOLOGICAL STRUCTURES, PREBIOL
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ORAL PRESENTATIONS
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OP‐1developed a theory of the gre
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OP‐2field of the Sun and the fiel
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OP‐3HOT ABIOGENESIS AND EARLY BIO
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OP‐4acetic acid [5,6], acetonitri
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OP‐6processes. Mentioned above as
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OP‐7polymerization of simple mole
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OP‐9SYNTHESIS OF BIOLOGICALLY IMP
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OP‐11threshold is reached the sel
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OP‐12nanoparticles of polysilicic
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OP‐13We aimed to relate entropy m
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OP‐14gene sequence as about 100 M
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OP‐15of photochemical transformat
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OP‐16modeled by the varying of in
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OP‐17[2]. Mulkidjanian, A. Y., Ko
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OP‐19LIFE ORIGINATION HYDRATE HYP
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OP‐20PREBIOLOGICAL EVOLUTION OF M
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OP‐21The manifestation of this ge
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OP‐22dominated by ostracodes, fir
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OP‐23present as Fe 0 , Fe +2 , an
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PROCARYOTIC ASSEMBLAGES OF EARLY PR
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OP‐26OPTIMIZATION OF STRESS RESPO
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OP‐27LICHENS COULD BE RESPONSIBLE
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OP‐28ROLE OF CYANOBACTERIA FROM D
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OP‐29COMPUTER TOOL FOR MODELING T
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OP‐30EVOLUTION OF TRANSLATION TER
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WHY WE NEED NEW EVIDENCES FOR DEEP
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ENDEMIC GENERA IN LATITUDINAL FAUNI
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OP‐33Taxonomic structure (alpha d
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OP‐34populations of different gas
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OP‐36in the reef frame, thus incr
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OP‐37extracorporeal digestion. Pl
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97OP‐38
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OP‐39one of the major generalized
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OP‐40geological history was favor
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“BUTTERFLY EFFECT” IN PLANETESI
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OP‐44COEVOLUTION OF MAMMALIAN FAU
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FRAMEWORKS OF LIFE ORIGIN RESEARCH
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OP‐45[8]. Lincoln T.A., Joyce G.F
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to run the analysis. Lifeless conde
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the pairs of the “very first” (
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aromatic hydrocarbons (PAHs) and th
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Results: Considering the changes be
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PP‐67ADAPTATION OF THE PYROCOCCUS
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GROWTH OF MICROORGANISMS IN MARTIAN
Page 124 and 125: 2.3. Cellular thalli (or colonies?)
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Page 128 and 129: A FRACTAL SPATIOTEMPORAL STRUCTURE
Page 130 and 131: [13]. Gusev, V.A., Arithmetic and a
Page 132 and 133: ABIOGENIC SELF‐ASSEMBLAGE OF THE
Page 134 and 135: PP‐2FLUID INCLUSION IN QUARTZ FRO
Page 136 and 137: PP‐3PALEOZOIC APOCALYPSE: WHAT CA
Page 138 and 139: PP‐4BIOCHEMICAL REACTION OF EARLY
Page 140 and 141: PP‐5EDIACARAN SOFT‐BODIED ORGAN
Page 142 and 143: PP‐6SOFTWARE MODELLER OF EVOLUTIO
Page 144 and 145: PP‐8THE EARLIEST STEPS OF ORGANIS
Page 146 and 147: PP‐9MODELING THE CONFIGURATIONS O
Page 148 and 149: PP‐9Acknowledgement. This work wa
Page 150 and 151: PP‐10that are much darker (probab
Page 152 and 153: PP‐12GTF2I DOMAIN: STRUCTURE, EVO
Page 154 and 155: PP‐13DEEP INSIDE INTO VERTEBRATES
Page 156 and 157: GENERATION OF MODERN MINERAL‐BIOL
Page 158 and 159: ADSORPTION OF RIBOSE NUCLEOTIDES ON
Page 160 and 161: PP‐16cells. Thus, in addition to
Page 162 and 163: PP‐17organizing photosynthetic pi
Page 164 and 165: PP‐19YOUNGEST OIL OF PLANET EARTH
Page 166 and 167: PP‐20MID‐CHAIN BRANCHED MONOMET
Page 168 and 169: PP‐21BIOMARKER HYDROCARBON COMPOS
Page 170 and 171: PP‐22BIOMARKER HYDROCARBONS IN KA
Page 172 and 173: PP‐23EVOLUTION OF TRILOBITE BIOFA
Page 176 and 177: CYANO‐BACTERIAL MATS OF HOT SPRIN
Page 178 and 179: PP‐26THE BIOGEOGRAPHICAL EVOLUTIO
Page 180 and 181: PP‐27MICROBIAL COMMUNITIES OF OIL
Page 182 and 183: PP‐28MICROEVOLUTIONARY PROCESSES
Page 184 and 185: BIOGENIC AND ABIOGENIC BIOMORPHIC S
Page 186 and 187: PP‐29are combine nodules forming
Page 188 and 189: PP‐30have led to divergence of la
Page 190 and 191: PP‐31observed in the modern micro
Page 192 and 193: PP‐32by the ammonite Arctocephali
Page 194 and 195: PP‐33similarities in their three
Page 196 and 197: PP‐34been formed already in the e
Page 198 and 199: PP‐35The epochs of global cooling
Page 200 and 201: PP‐37MULTIPLE PATHS TO ENCEPHALIZ
Page 202 and 203: PP‐38FIRST MIKROIHNOFOSSILS FIND
Page 204 and 205: PP‐39THE ROLE OF ECHINOIDS IN SHA
Page 206 and 207: PP‐40BIOMARKER HYDROCARBONS OF TH
Page 208 and 209: THE STRUCTURE OF MICROBIAL COMMUNIT
Page 210 and 211: PP‐42Plate 1. Middle Ordovician,
Page 212 and 213: PP‐43ecosystems of large (up to 6
Page 214 and 215: PP‐44expansion goes through 40 °
Page 216 and 217: PP‐45(Ketris and Judovich, 2009),
Page 218 and 219: SURVIVAL OF HALOPHILES AT DIFFERENT
Page 220 and 221: PP‐47ISOPRENOID BIOMARKERS AND MI
Page 222 and 223: SOME PECULIARITIES IN THE DISTRIBUT
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PP‐51EVOLUTION OF INFAUNAL SCAVEN
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PP‐52EARLY PROTEROZOIC BIOMORPHIC
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PP‐53FROM OFFSHORE TO ONSHORE:A N
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PRODUCTS FROM BIRCH BARK FOR TREATI
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PP‐55THE STRUCTURE OF MICROBIAL C
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233PP‐56
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PP‐58EARLY CAMBRIAN EVOLUTION OF
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PP‐59matter (OM) of the Kuonamka
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PP‐60Fig. 1. Masschromatograms fo
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PP‐61multiply. According to prof.
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PP‐62investigation of dietary pat
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PP‐63for almost all discs. Radial
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PP‐64BIOMARKERS IN PRECAMBRIAN KA
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MICROFOSSILS OF BACTERIAL, MUSHROOM
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PP‐66BIOSTRUCTURE OF ASSEMBLAGES
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Abramson Natalia IosifovnaZoologica
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Gerasimov MikhailSpace Research Ins
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Lomakina AnnaLimnological institute
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Rogov Vladimir IgorevichTrofimuk In
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Zamulina Tatiana VladimirovnaBoresk
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PL‐9Kolchanov N.A., Afonnikov D.A
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OP‐15Gontareva N.B., Kuzicheva E.
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OP‐33Barskov I.S.TAXONOMICAL AND
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Nagovitsin K.COMPLEX HETEROTROPHIC
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PP‐17.PP‐18.PP‐19.PP‐20.PP
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PP‐35.Polishchuk Y.M., Yashchenko
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PP‐54.PP‐55.Kuznetsova S.A.PROD
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III INTERNATIONAL CONFERENCEBIOSPHE
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